scholarly journals I. On the organisation of the fossil plants of the coal-measures; Part XVI

1889 ◽  
Vol 45 (273-279) ◽  
pp. 438-440

In this memoir the author first calls attention to detached observa­tions made in his earlier memoirs relating to the manner in which a medullary axis is developed in the interior of each of the primary vascular bundles of the Carboniferous Lycopodiacæ.

1888 ◽  
Vol 44 (266-272) ◽  
pp. 367-368

The author describes and figures a series of specimens which throw new light upon Corda’s two genera Zygopteris and Anachoropteris , as they are adopted by M. Renault, but which specimens show that both these genera can no longer be retained, even by those who approve of such multiplications of ill-defined genera. He proposes, therefore, the abandonment of Anachoropteris and the retention of Zygopteris , so that " Zygopteroid " may be employed as a descriptive adjective in connexion with some specially remarkable forms of petiolar vascular bundles.


In the fourth of this series of Memoirs (‘Phil. Trans.,' 1873, p. 377, et seq .) I described a remarkable plant under the name of Dictyoxylon Oldhamium ; I also gave reasons for substituting the late Mr. Gourlie ’s generic name of Lyginodendron for that of Dictyoxylon . In the same Memoir (p. 403) I referred to some petioles, to which I proposed to assign the name of Edraxylon ; but later researches demonstrated the necessity for abandoning this as a generic term and substituting for it the more comprehensive one of Rachiopteris aspera . In my Memoir, Part VI. ('Phil. Trans.,' 1874, Plate 2, p. 679, et seq .), I described this proposed Edraxylon under the name of Rachiopteris aspera . Certain similar features exhibited by the above two plants led me to remark in Memoir IV., p. 403, after showing that the Rachiopteris aspera was obviously the petiole of a Fern, “I think it far from impossible that these may prove to belong to Dictyoxylon ( Lyginodendron ) Oldhamium ; but since I have not yet succeeded in correlating them with any certainty, 1 shall add no more respecting them at present.” Since 1873 1 have accumulated a vast amount of material illustrative of the structure and relations of these two plants, and am now in a position to demonstrate that they respectively represent the stem and petiole of the same organism which proves to be a Fern. I was long under the conviction that the remarkable exogenous development of the stems of many of the Carboniferous Cryptogams, which I have so continuously demonstrated to exist, and which is now so universally recognised by Palæontologists, had no existence amongst Ferns. I have now to show that this development did exist amongst Ferns as well as amongst the arborescent Lycopods and Calamites, in which it is so conspicuous. Fig. 1 (Plate 12) is part of a transverse section of a stem or branch of Lyginodendron Oldhamium , in which a represents the medulla; b , the exogenous xylem zone; c , the place of the inner cortex, wanting in this specimen; d , one of the pairs of vascular bundles, so characteristic of the, cortex of this plant; e , the outermost cortex, composed, in transverse sections, of radiating bands of sclerenchyma, g , alternating with parenchymatous areas, f . At k, k we find two bundles of tracheids, like those at d , forming the centre of the cortical structures of a petiole of Rachiopteris aspera , i, i , which petiole is organically united to the cortex e of the Lyginodendron . The two bundles k, k are assuming the oblique relative positions seen in the similar bundles of the free petiole of R. aspera , represented in fig. 2. Other sections in my cabinet, similar to fig. 1, demonstrate the same facts, viz., that the pairs of bundles, fig. 1, d , which form so characteristic a feature of transverse sections of the middle cortex of Lyginodendrom Oldhamium , pass outwards, through the outer cortex, to become the tracheæal bundles of the petioles of the plant, and which petioles I had previously designated Rachiopteris aspera . I may state that my friend Graf Solms-Laubach, who has obtained numerous specimens of the Lyginodendron associated with others of Rachiopteris aspera from a locality on the continent, agrees with me in the conclusion at which I have arrived respecting their unity. The more perfect specimens of the Lyginodendron obtained during the last seventeen years have thrown yet further light upon those figured in 1873. In the latter, as at fig. 1, c, no traces of the middle bark were preserved; but examples from Halifax, for which I am indebted to my friends Mr. Cash and Mr. Spencer, of Halifax, have supplied what was wanting. Fig. 3 is a transverse section in which this inner cortex, c , is shown to consist of a zone of extremely delicate, thin-walled parenchymatous cells, scattered throughout which are numerous gum-canals, l . Three of these canals are represented, enlarged 250 diameters, in figs. 4 and 5, embedded in the thin-walled cells, c, c , of the cortex.


1874 ◽  
Vol 22 (148-155) ◽  
pp. 248-251

The author called attention to the various methods of classifying the fern-stems and petioles of the Coal-measures adopted by Cotta, Corda, Brongniart, and others, and to the difficulties which attend those methods. Some of those difficulties had been already felt and partially removed by M. Brongniart. All the generic distinctions hitherto adopted were based upon variations in the form, number, and arrangement of the vascular bundles. These elements vary so much, not only in different species of the same genus, but in different parts of the same petiole, as to make them most untrustworthy guides to generic distinctions. The consequence has been an enormous multiplication of genera; but, notwithstanding their number, the author found that if he adopted the methods of his predecessors he would have to establish additional ones for the reception of his new forms. Under these circumstances he decides that it will be better to include the entire series of these petioles, provisionally, under the common generic term of Rachiopteris . This plan dispenses with a number of meaningless genera, and is rendered additionally desirable by the circumstance that ah the petioles to which these numerous generic names have been applied belong to fronds which have already received other names, such as Pecopteris, Sphenoteris , &c., only the structure of fronds found in the shales, and their respective petioles of which we have ascertained the structure, have not yet been correlated. As a preparation for the present investigation, the author made an extensive series of researches amongst recent British and foreign fern-stems and petioles, with the object of ascertaining not only the modifications in their arrangements in different parts of the same plant, but especially of studying the modes in which secondary and tertiary vascular bundles were derived from the primary ones. This inquiry led him over the ground previously traversed by M. Trécul, and, so far as British ferns were concerned, by Mr. Church.


1872 ◽  
Vol 20 (130-138) ◽  
pp. 95-96

My dear Dr. Sharpey,—Since I read my last communication to the Royal Society on the organization of the Fossil Plants of the Coal-measures I have done a large amount of work, having cut between two and three hundred new sections and with most satisfactory results. I have obtained a series of specimens almost completing the life-history of one plant from Burntisland, beginning with the tips of the smallest twigs and ending with the large stems. The former are mere aggregations of parenchyma with a central bundle of barred vessels mixed with a small amount of primitive cell-tissue. As the twig grew the leaves assumed definite form, and the central vascular bundle opened out at its central part, so as to form a cylinder, the interior of which was occupied by parenchyma. This cylinder grew rapidly, the number of its vessels steadily increasing; but they were all equally arranged as in, what I have termed, the medullary vascular cylinder, i. e. not in radiating series. We thus obtain the origin of that remarkable cylinder, and see that it is the expanded homologue of the central vascular bundles of the living Lycopods. Whilst these processes were in progress the cortical portion became differentiated into layers, and the parenchymatous cells of the pith continued to multiply, so as to occupy the expanding interior of the vascular cylinder. After attaining a certain size, through the above processes, a new element of growth appeared; an exogenous addition was made to the exterior of the cylinder, also consisting of barred vessels, but these are arranged in the radiating series described in my last memoir. This series continued to grow until it attained to considerable dimensions; but the entire vascular system always remains small, compared with the diameter of the stem, the chief bulk of which consists of an enormously thick bark. The structure just descibed is that of a true example of the genus Diploxylon of Corda. But I have got abundance of specimens with leaves on the exterior of the bark, demonstrating that the plant is a true Lomatophloios , thus indicating the correctness of my supposition, advanced in my last memoir, that sooner or later the genus Diploxylon would have to be abandoned.


1871 ◽  
Vol 19 (123-129) ◽  
pp. 500-504

The Lepidodendron selaginoides described by Mr. Binney, and still more recently by M r. Carruthers, is taken as the standard of comparison for numerous other forms. It consists of a central medullary axis composed of a combination of transversely barred vessels with similarly barred cells; the vessels are arranged without any special linear order. This tissue is closely surrounded by a second and narrower ring, also of barred vessels, but of smaller size, and arranged in vertical laminae which radiate from within outwards. These laminae are separated by short vertical piles of cells, believed to be medullary rays. In the transverse section the intersected mouths of the vessels form radiating lines, and the whole structure is regarded as an early type of an exogenous cylinder; it is from this cylinder alone that the vascular bundles going to the leaves are given off.


1880 ◽  
Vol 171 ◽  
pp. 493-539 ◽  

In 1865 my friend Mr. Edward Wunsch, of Glasgow, made the discovery of some thin carboniferous shales imbedded in volcanic ash at Laggan Bay, in Arran. These beds have already been described by their discoverer, and their fossil contents referred to by Mr. Binney, Mr. Carruthers, and Sir Charles Lyell. From within a very limited area the bases of more than 13 large erect stems of carboniferous trees have been extracted by Mr. Wunsch, the most important of which he has kindly placed in my hands. In the summer of 1877 we conjointly superintended some quarrymen, who tore up large portions of these strata with the result, I believe, of obtaining a fair knowledge of the nature of these beds and their contents. The trees certainly stood where they originally grew; most of them consisted of a thin cylinder of the outer bark, which was deeply fissured longitudinally but exhibited no true Sigillarian flutings or traces of leaf-scars. The interior was in most cases filled with volcanic ash, but in a few instances by vegetable débris introduced from without; and in one specimen, imbedded in the vegetable mass, are several decorticated Diploxyloid vascular axes of very old stems. These have been referred to as young growths that sprang up within the bark-cylinder; but such is not the case. Each one is not only decorticated, but is large enough to be the vascular axis of the large tree within which the entire group occurs, and where they are mixed up with fragments of the similar vascular axes of Stigmaria and other plants.


1928 ◽  
Vol 65 (8) ◽  
pp. 356-363 ◽  
Author(s):  
Emily Dix ◽  
A. E. Trueman

The fossils of the Coal Measures of South Wales have probably not been studied so systematically or for so many years as those of certain coalfields of he north of England, and it is only within recent years that any marked progress has been made in their investigation; this is especially true of the marine fossils.


1889 ◽  
Vol 180 ◽  
pp. 195-214 ◽  

During the last twenty years many single examples of vegetable forms from Carboniferous rocks have come into my possession, which were obviously different from any hitherto described. But I have carefully abstained from publishing such specimens until examples of each multiplied in my cabinet, enabling me to determine how far their apparently distinctive features were constant, and not merely individual, variations. Many such imperfectly known forms still occupy a drawer in my cabinet; but in the present Memoir I propose to describe several of which examples have accumulated so far as to enable me to speak with reasonable certainty as to their specific distinctiveness. In several of my previous memoirs I have from time to time called attention to a curious development of a medulla in the centre of the axial vascular bundle, especially of the Lepidodendra. This was especially done in the Memoir, Part III., when describing the Burntisland Lepidodendron , to which, as was also the case with the Arran form (Part X.), I have not yet ventured to give a specific name.


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